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FIG. 3 in Les hétéroptères (Insecta, Hemiptera) décrits par Paul Dispons. Inventaire commenté des spécimens types conservés au Muséum national d'Histoire naturelle, Paris

FIG. 3. — Carton et spécimens de la collection Dispons montrant les modes de préparation et deux exemples de paillettes non standard confectionnées par Dispons; A, carton d'Harpactorinae renfermant des spécimens de diverses provenances (Asie, Afrique), la plupart non identifiés; B, Jamesa chabaunaudi frater Dispons, 1969, holotype; C, Jamesa uelensis aequalis Dispons, 1969, holotype.

FIG. 2 in Les hétéroptères (Insecta, Hemiptera) décrits par Paul Dispons. Inventaire commenté des spécimens types conservés au Muséum national d'Histoire naturelle, Paris

FIG. 2. — Aspects insolites de la collection Dispons: les pontes et descendances de femelles ont toujours été soigneusement conservées par l'auteur: A, Rhinocoris erythropus (Linnaeus, 1767), ponte sur fragment végétal, oeufs et opercules; B, idem, ponte; C, Coranus sp., immatures de stades 1, 2 et 3.

FIG. 1 in Les hétéroptères (Insecta, Hemiptera) décrits par Paul Dispons. Inventaire commenté des spécimens types conservés au Muséum national d'Histoire naturelle, Paris

FIG. 1. — Portrait de Paul Dispons en 1949 (photo: ministère de la Défense, SHD, Armée de Terre, cote 15 Yd 1064).

FIG. 4. — Photographie d in Les hétéroptères (Insecta, Hemiptera) décrits par Paul Dispons. Inventaire commenté des spécimens types conservés au Muséum national d'Histoire naturelle, Paris

FIG. 4. — Photographie d'une page du registre de chasse de P. Dispons correspondant à des récoltes faites en avril 1954 dans le Sud marocain (Tiznit, Arak).

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Figure 14 Type locations. A in Paraquanothrus n. gen. from freshwater rock pools in the USA, with new diagnoses of Aquanothrus, Aquanothrinae, and Ameronothridae (Acari, Oribatida)

Figure 14 Type locations. A – type location of Paraquanothrus grahamin. sp., on barren sandstone ('slickrock fin') near Moab, Utah; B – same, closeup of dry 'pan' (shallow rock pool; cell phone and∼15 cm ruler for scale); C – same general location, small water-filled pan containing more than 100 individuals∼(10 cm pipette for scale); D-F – type location of Paraquanothrus spoonerin. sp., Heggie's Rock, Georgia, general view (D) and small dry rock pools (E-F) containing mites, vegetated by Black Rock Moss (Grimmia laevigata(Bird.)) and Elf Orpine (Diamorpha smalliiBritton ex Small). Photographs contributed by Tim Graham (A-C) and John Spooner (D-F).

FIG. 4 in On type material and the identity of several Iulus species described by Paul Gervais, in the collection of the Muséum national d'Histoire naturelle in Paris (Diplopoda, Spirostreptida, Spirobolida)

FIG. 4. — Neocricus striolatus (Gervais, 1847), holotype; A, gonopods (front view); B, anterior gonopods (caudal view); C, D, left posterior gonopod (lateral and mesal, respectively). Scale bar: 2.0 mm.

FIG. 3 in On type material and the identity of several Iulus species described by Paul Gervais, in the collection of the Muséum national d'Histoire naturelle in Paris (Diplopoda, Spirostreptida, Spirobolida)

FIG. 3. — Amastigogonus verreauxii (Gervais, 1847), holotype; A, anterior body end (lateral view); B, midbody segment (lateral view); C, telson (lateral view); D, leg-pair 1 and gnathochilarium (caudal view); E, gonopods (caudal view); F, G, anterior gonopod (front and lateral views, respectively); H, left posterior gonopod (caudal view). Scale bars: A-D, 1.0 mm; E-H, 0.5 mm.

FIG. 2 in On type material and the identity of several Iulus species described by Paul Gervais, in the collection of the Muséum national d'Histoire naturelle in Paris (Diplopoda, Spirostreptida, Spirobolida)

FIG. 2. — Gymnostreptus trimarginatus (Gervais, 1847), lectotype; A, anterior body end (lateral view); B, midbody segment (lateral view); C, telson (lateral view). Scale bar: 2.0 mm.

FIG. 1 in On type material and the identity of several Iulus species described by Paul Gervais, in the collection of the Muséum national d'Histoire naturelle in Paris (Diplopoda, Spirostreptida, Spirobolida)

FIG. 1. — Gymnostreptus sublaevis (Gervais, 1847), lectotype (A, C-H) and female paralectotype (B); A, collum (lateral view); B, telson (lateral view); C, gena (lateral view); D, leg 1 (front view); E-G, gonopods (front, lateral, and caudal views, respectively, with lateral folds of paracoxites broken off); H, tip of solenomerite (drawn not to scale). Scale bars: A-G, 2.0 mm; H, 1.0 mm.

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Text-fig. 6. Scanning electron micrographs of multicarpellate and apocarpous floral structures from the Early Cretaceous Puddledock locality, Virginia, USA (a, b: PP43701, Puddledock sample 001; c: PP43000x, Puddledock sample 073). a) Anacostia? sp., strongly compressed, elongated receptacle with spirally arranged carpels (red dots; not all shown); note larger size compared to the other floral structures; b) Numerous Anacostia type pollen grains in proximal view from the base of floral structure in (a); note graded reticulum over the proximal pole of the pollen grains; c) Elongated receptacle with numerous carpels in a spiral arrangement, possibly representing an earlier developmental stage of Anacostia? sp. Scale bars = 1 mm (a, c), 10 µm (b). in Multiparted, Apocarpous Flowers From The Early Cretaceous Of Eastern North America And Portugal

Text-fig. 6. Scanning electron micrographs of multicarpellate and apocarpous floral structures from the Early Cretaceous Puddledock locality, Virginia, USA (a, b: PP43701, Puddledock sample 001; c: PP43000x, Puddledock sample 073). a) Anacostia? sp., strongly compressed, elongated receptacle with spirally arranged carpels (red dots; not all shown); note larger size compared to the other floral structures; b) Numerous Anacostia type pollen grains in proximal view from the base of floral structure in (a); note graded reticulum over the proximal pole of the pollen grains; c) Elongated receptacle with numerous carpels in a spiral arrangement, possibly representing an earlier developmental stage of Anacostia? sp. Scale bars = 1 mm (a, c), 10 µm (b).

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Text-fig. 6. The riparian/swamp forest structure of the village of Sakarcaören in the late Miocene, location within the east part of GVP, and comparison with the other forest types from early Miocene of GVP (Akkemik et al. 2009, 2016, 2017, Bayam et al. 2018). in The First Glyptostroboxylon And Taxodioxylon Descriptions From The Late Miocene Of Turkey And Palaeoclimatological Evaluation

Text-fig. 6. The riparian/swamp forest structure of the village of Sakarcaören in the late Miocene, location within the east part of GVP, and comparison with the other forest types from early Miocene of GVP (Akkemik et al. 2009, 2016, 2017, Bayam et al. 2018).

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Text-fig. 5. Scanning electron microscope (SEM) images of megaspores with possible affinities to Isoetales (a–d) and megaspores of uncertain affinity (e–i); Torres Vedras locality, Portugal. a) Paxillitriletes reticulatus megaspore in lateral view showing long appendages on the flanges of the laesurae and the reticulate-spiny distal surface; b) Dijkstraisporites sp. megaspore in oblique lateral view showing long, sometimes dichotomizing, appendages on the equatorial flanges and bordering the laesurae; c, d) Tenellisporites sp. megaspore in proximal view (c) showing equatorial flanges and laesurae with short, broad, flattened and unbranched appendages; note numerous, spiny microspores adhering to the proximal face of the megaspore (d); e) Megaspore type sp. 2 in lateral view showing apical gula and ornamentation of scattered spines; f, g) Megaspore type sp. 3 in lateral (f) and proximal (g) view showing broad, often dichotomously branched appendages covering the megaspore surface; h, i) aff. Flabellisporites sp. megaspores in proximal (h) and lateral (i) view showing long, narrow appendages covering the megaspore surface. Specimens, TV39-S174619 (a), TV38-S170220 (b), TV38-S170221 (c, d), TV44-S174574 (e), TV44-S174575 (f), TV44-S174577 (g), TV38-S170223 (h), TV38-S170222 (i). Scale bars 100 Μm (a–c, e–i), 25 Μm (d). in The Early Cretaceous Mesofossil Flora Of Torres Vedras (Ne Of Forte Da Forca), Portugal: A Palaeofloristic Analysis Of An Early Angiosperm Community

Text-fig. 5. Scanning electron microscope (SEM) images of megaspores with possible affinities to Isoetales (a–d) and megaspores of uncertain affinity (e–i); Torres Vedras locality, Portugal. a) Paxillitriletes reticulatus megaspore in lateral view showing long appendages on the flanges of the laesurae and the reticulate-spiny distal surface; b) Dijkstraisporites sp. megaspore in oblique lateral view showing long, sometimes dichotomizing, appendages on the equatorial flanges and bordering the laesurae; c, d) Tenellisporites sp. megaspore in proximal view (c) showing equatorial flanges and laesurae with short, broad, flattened and unbranched appendages; note numerous, spiny microspores adhering to the proximal face of the megaspore (d); e) Megaspore type sp. 2 in lateral view showing apical gula and ornamentation of scattered spines; f, g) Megaspore type sp. 3 in lateral (f) and proximal (g) view showing broad, often dichotomously branched appendages covering the megaspore surface; h, i) aff. Flabellisporites sp. megaspores in proximal (h) and lateral (i) view showing long, narrow appendages covering the megaspore surface. Specimens, TV39-S174619 (a), TV38-S170220 (b), TV38-S170221 (c, d), TV44-S174574 (e), TV44-S174575 (f), TV44-S174577 (g), TV38-S170223 (h), TV38-S170222 (i). Scale bars 100 Μm (a–c, e–i), 25 Μm (d).

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Text-fig. 21. Scanning electron microscope (SEM) images of stamens (a–c) with in situ trichotomocolpate Asteropollis type pollen (d– h); Torres Vedras locality, Portugal. a) Fragmentary tetrasporangiate stamen; b) Group of tetrasporangiate stamens; c) Single pollen sac from stamen; d, f) Distal view of pollen grains showing trichotomocolpate aperture; e, g) Pollen wall showing dense reticulum with faint supratectal ornamentation; h) Detail of pollen wall showing numerous long columellae. Specimens, TV44-S105012 (a, d), TV44-105015 (b, e), TV44-S136763 (c, f, g), TV44- S136669 (h). Scale bars 300 Μm (a–c), 6 Μm (d, f), 1.5 Μm (e, g, h). in The Early Cretaceous Mesofossil Flora Of Torres Vedras (Ne Of Forte Da Forca), Portugal: A Palaeofloristic Analysis Of An Early Angiosperm Community

Text-fig. 21. Scanning electron microscope (SEM) images of stamens (a–c) with in situ trichotomocolpate Asteropollis type pollen (d– h); Torres Vedras locality, Portugal. a) Fragmentary tetrasporangiate stamen; b) Group of tetrasporangiate stamens; c) Single pollen sac from stamen; d, f) Distal view of pollen grains showing trichotomocolpate aperture; e, g) Pollen wall showing dense reticulum with faint supratectal ornamentation; h) Detail of pollen wall showing numerous long columellae. Specimens, TV44-S105012 (a, d), TV44-105015 (b, e), TV44-S136763 (c, f, g), TV44- S136669 (h). Scale bars 300 Μm (a–c), 6 Μm (d, f), 1.5 Μm (e, g, h).

Text-fig. 20. ONHM TN 2017-01, anthracothere 1st phalanx in situ in indurated marl at the Omanitherium type locality. in Large Mammals From The Rupelian Of Oman - Recent Finds

Text-fig. 20. ONHM TN 2017-01, anthracothere 1st phalanx in situ in indurated marl at the Omanitherium type locality.

Text-fig. 8. Lower teeth of Arsinoitherium andrewsi from the Omanitherium type locality, Ashawq Formation, Oman. a) ONHM TN 2017-03, right m/3, (a1 – stereo buccal view, a2 – stereo occlusal view); b) ONHM TN 2017-04, right p/2 (b1 – stereo buccal view, b2 – stereo occlusal view); c) ONHM TN 2017-06, right p/4 (c1 – stereo buccal view, c2 – stereo occlusal view) (scale bar 10 mm). in Large Mammals From The Rupelian Of Oman - Recent Finds

Text-fig. 8. Lower teeth of Arsinoitherium andrewsi from the Omanitherium type locality, Ashawq Formation, Oman. a) ONHM TN 2017-03, right m/3, (a1 – stereo buccal view, a2 – stereo occlusal view); b) ONHM TN 2017-04, right p/2 (b1 – stereo buccal view, b2 – stereo occlusal view); c) ONHM TN 2017-06, right p/4 (c1 – stereo buccal view, c2 – stereo occlusal view) (scale bar 10 mm).

Text-fig. 5. Upper part of the stratigraphic section at the Omanitherium type locality. B–D correspond to the beds identified in the stratigraphic section (Text-fig. 3). The workers are excavating at the type locality. in Large Mammals From The Rupelian Of Oman - Recent Finds

Text-fig. 5. Upper part of the stratigraphic section at the Omanitherium type locality. B–D correspond to the beds identified in the stratigraphic section (Text-fig. 3). The workers are excavating at the type locality.

Text-fig. 7. Steinkerns of the land snail Arabicolaria omanensis eroding from indurated dark green-brown sands of Bed C above the Omanitherium type locality (the pen is 14.5 cm long). in Large Mammals From The Rupelian Of Oman - Recent Finds

Text-fig. 7. Steinkerns of the land snail Arabicolaria omanensis eroding from indurated dark green-brown sands of Bed C above the Omanitherium type locality (the pen is 14.5 cm long).

Text-fig. 4. Measured section at the Omanitherium type locality. A–D are indurated beds highlighted in the stratigraphic section (figure seated on outcrop B provides a scale) (see Text-fig. 3). in Large Mammals From The Rupelian Of Oman - Recent Finds

Text-fig. 4. Measured section at the Omanitherium type locality. A–D are indurated beds highlighted in the stratigraphic section (figure seated on outcrop B provides a scale) (see Text-fig. 3).

Text-fig. 3. Stratigraphic section through part of the Ashawq Formation at the Omanitherium type locality, Dhofar Governorate, Oman. Beds A–D are indurated cliff-forming strata identified in the accompanying field photographs (Textfigs 4, 5). Note the increase in marine influence as one ascends through the section, the fauna in Beds A and B being dominated by freshwater molluscs and land snails, with few brackish water specimens, whereas the biota in Bed D is frankly marine with a single specimen of the freshwater snail Pila. Bed C yielded Vermetus, oysters and sponges, but also contains abundant land snails and a low diversity of freshwater gastropods. in Large Mammals From The Rupelian Of Oman - Recent Finds

Text-fig. 3. Stratigraphic section through part of the Ashawq Formation at the Omanitherium type locality, Dhofar Governorate, Oman. Beds A–D are indurated cliff-forming strata identified in the accompanying field photographs (Textfigs 4, 5). Note the increase in marine influence as one ascends through the section, the fauna in Beds A and B being dominated by freshwater molluscs and land snails, with few brackish water specimens, whereas the biota in Bed D is frankly marine with a single specimen of the freshwater snail Pila. Bed C yielded Vermetus, oysters and sponges, but also contains abundant land snails and a low diversity of freshwater gastropods.